A Okamoto, R Oyanagi - Progress in Earth and Planetary Science, 2023 - Springer
The slab–mantle interface in subduction zones is one of the geological boundaries with the most significant chemical potential gradients, which leads to fluid-mediated metasomatic …
C Herviou, G Bonnet - Geochemistry, Geophysics, Geosystems, 2023 - Wiley Online Library
Meter‐to hectometer‐size horizons of carbonate‐bearing talcschists are found along or near the contacts between the different Liguro‐Piemont subduction slices. Through mineral and …
Metasomatism of the subducting slab and mantle wedge influences the rheological and chemical properties of rocks at the subduction zone interface. We investigated a serpentinite …
Talc‐rich rocks are common in exhumed subduction zone terranes and may explain geophysical observations of the subduction zone interface, particularly beneath Guerrero …
Slow earthquakes, including low-frequency earthquakes, tremor, and geodetically detected slow-slip events, have been widely detected, most commonly at depths of 40–60 km in …
C Herviou, P Agard, A Verlaguet… - Journal of …, 2023 - Wiley Online Library
Abstract In the Western Alps, oceanic lithosphere fragments recovered from subduction are exposed continuously across the Liguro‐Piemont domain. In this nappe‐stack, the Schistes …
The shallow segment of subduction plate boundary faults (< 10 km) hosts diverse slip modes including low-frequency earthquakes and slow slip. These slip behaviors are thought to be …
The shallow segment of subduction plate boundary faults (< 10 km) hosts diverse slip modes including low-frequency earthquakes and slow slip. These slip behaviors are thought to be …